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Megaearthquake of March 11, 2011, in Japan: The Event Magnitude and the Character of the Aftershock Sequence

机译:2011年3月11日在日本发生的特大地震:震级和余震序列的特征

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摘要

The great Japanese earthquake (GJE) of March 11, 2011, was a megaevent. The conditions under which such seismic catastrophes occurred are discussed. The regime of the aftershocks of this megaevent is compared with the data on the aftershock sequences which accompanied the Simushir earthquakes (2006 and 2007) and the Andaman earthquake (2004) and with the seismicity behavior in the generalized vicinity of a strong earthquake. The aftershock sequences of the abovementioned strong earthquakes are shown to represent the sets of trend changes in the postshock activity and specific outbursts of seismic activity. Activity outbursts are characterized not only by an increase in the number and energy of events, but also by a decrease in the recurrence plot slope (b value) and the average earthquake depth. Some such outbursts correspond to the occurrence of strong repeated shocks. A possible mechanism for outbursts of seismic activity is proposed. The possibility ofa stronger repeated shock in the vicinity ofthe megaearthquake of March 11, 2011, is discussed.
机译:2011年3月11日的日本大地震(GJE)是一个大事件。讨论了发生此类地震灾难的条件。将这一特大事件的余震状态与伴随Simushir地震(2006年和2007年)和Andaman地震(2004年)的余震序列数据以及在强地震普遍性附近的地震活动性进行了比较。上面提到的强地震的余震序列显示为代表了震后活动和地震活动特定爆发的趋势变化集。活动爆发的特征不仅在于事件数量和能量的增加,还在于递归图斜率(b值)和平均地震深度的减小。一些这样的爆发对应于强烈的反复震动的发生。提出了一种可能的地震活动爆发机制。讨论了在2011年3月11日的特大地震附近发生更大的反复震动的可能性。

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